The karst hides unrevieled and hardly accesible treasure in its underground - water, pits, caves and animals.
Vertical hollows with steep sides, mainly of small diameters and great depths are the characteristics of this part of the Velebit mountain. These karst holes are called PITS. They were formed by joined efforts of inner and outer forces of nature (tectonics and water). Through the centuries, these pits were considered to have supernatural forces. They evoked fear and respect at the indigenous population, but also gratitude for snow and water which could often be found inside them during the hot summer months.
Many of these pits were named after some tragical events from long ago, like the Crna snježnica ("Black Snowpit") on the Pivčevac peak. Many tales and legends of this land are directly connected to pits.
The Italian priest Alberto Fortis wrote in one of his essays about Velebit in 1774. that "bura" - the cold northern wind - generates in the Velebit's underground and finds its way out through the pits.
The first description of the pits of northern Velebit was made by the geologist Josip Poljak in 1929. He described Vukušić-icepit, Varnjača hole and Hajduk cave. The same year, Ante Premužić, Ivan Krajač and Marko Vukelić descend in the hole of Varnjača, Crikvena and the Hajdučka cave.
Speleological expeditions were not continued until 1961., when systematical researches started. The explorations were intensified in the eighties, and it was not before the year 1992., when the famous Luke's pit was discovered, that this mountain started attracting numerous speleologists, advanturers and geologists. Due to this fact, in the last couple of years many new pits had been discovered.
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Until now, there are 178 speleological objects discovered on the area of the National Park (109 km2 ), most of which belong to the group of vertical underground holes, i.e. - pits.
Speleological objects in the Northern Velebit National Park
Pits owe their existance to the tectonic movements. These processes caused movements of huge rock masses either by raising, lowering or horizontal moving along the cracks called the paraclasis. Vaste rock masses cracked and broke in various directions.
Thus were formed the more or less shallow holes which directed downfalls straight into the underground, sometimes on great depths. Water influenced the carbon mineral rocks, melted them through millions of years and widened and broadened underground caves and holes.

The great number of pits on this relatively small area owe their existance greatly to the active tectonics. The movements that caused the Hajdučki and Rožanski Ledges to raise left their traces and formed pits which rank as some of the world's deepest, like the Luke's pit which is 1392 meters deep.
The newly discovered Velebita pit has the deepest verticale fall in the world - 553 meters.
Many of the recently discovered pits are not yet entirely explored. The assumption is that some pits are much deeper than they seem. Many speleological objects are yet to be discovered. Precise information about their depths and geological structure of the underground may provide us with some new knowldeges on the complex tectonics of this area.
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